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黑河流域上游降水精细化分布与总量年际变化
引用本文:孙佳,王可丽,江灏,雒新萍,朱庆亮.黑河流域上游降水精细化分布与总量年际变化[J].冰川冻土,2011,33(3):619-623.
作者姓名:孙佳  王可丽  江灏  雒新萍  朱庆亮
作者单位:1. 中国科学院 寒区旱区环境与工程研究所,甘肃 兰州 730000;中国科学院 研究生院,北京 100049
2. 中国科学院 寒区旱区环境与工程研究所,甘肃 兰州,730000
基金项目:国家自然科学基金项目(9102500540771006)资助
摘    要:利用黑河流域100 m×100 m地理地形资料及气象测站多年降水和风向资料,依据坡度、盛行风向与迎风坡对地形抬升速度影响的数学模式,对主导风向效应指数进行了扩展,构建了新的耦合坡度、坡向和主导风向的局地地形因子.通过回归分析,建立了逐年6-9月降水量与地理和局地地形因子的回归方程,通过GIS空间分析技术扩展得到了黑河流...

关 键 词:黑河流域  降水  精细化分布  总量  年际变化

The Elaborate Distribution of Precipitation and Interannual Variation of Total Precipitation in the Upstream of the Heihe River
SUN Jia,WANG Ke-li,JIANG Hao,LUOXin-ping,ZHU Qing-liang.The Elaborate Distribution of Precipitation and Interannual Variation of Total Precipitation in the Upstream of the Heihe River[J].Journal of Glaciology and Geocryology,2011,33(3):619-623.
Authors:SUN Jia  WANG Ke-li  JIANG Hao  LUOXin-ping  ZHU Qing-liang
Institution:SUN Jia1,2,WANG Ke-li1,JIANG Hao1,LUO Xin-ping1,ZHU Qing-liang1,2(1.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China,2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China)
Abstract:Using the geographical and topographic data with the resolution of 100 m×100 m and the meteorological observation data including precipitation and wind,in this paper,a new local terrain index of coupling slope,aspect and prevailing wind direction was constructed firstly based on the effect of prevailing wind direction and windward slope on precipitation,proposed by Fu Bayou,and the prevailing wind direction effect index,established by Sun Pengsen.The new index has more clear physical meanings of atmosphere-earth interaction.Then regression equations between precipitation from June to September and geographical and topographic factors were established by means of regression analysis year after year(1967—2008).According to the regression equations,the space elaborate distribution of precipitation from June to September can be obtained by spatial analysis year after year in the upstream.On this basis,the total precipitation can be calculated year after year in this area.The result showed that there were very good correlations between the new local terrain index and precipitation from June to September year after year.Cross test results showed that the regression equations can fit well the upstream precipitation.Especially since the late 1970s,the fitted values have been very close to the measured values.The average relative error was less than 10%.Based on the space elaborate distribution of the precipitation,the mean total precipitation from June to September was calculated to be about 98.2 billion m3 in the upstream of the Heihe River.The total precipitation had obviously interannual variation with a slight rising tendency.Before 1982,the total precipitation showed an ascendant tendency.During 1982 to 2000,the total precipitation fluctuated large.Since 2000,the total precipitation has increased obviously.
Keywords:Heihe River basin  precipitation  elaborate distribution  total amount  interannual variation  
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